Abstract
Time-dependent solutions of the diffusion and continuity equations are used to examine the diurnal variations of constituents in an oxygen-hydrogen atmosphere. Account has been taken of recent revisions in solar-flux data, predissociation of molecular oxygen in the Schumann-Runge bands, and experimental data on the height variation of the eddy diffusion coefficient. The results for O( 3P) , O 2, O 3 and O 2( 1Δ g) are compared with experimentally determined concentrations.
Published Version
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